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French multinational company and a world leader in the production and processing of industrial minerals, serving a wide range of high-performance industrial applications. This PhD project is part of
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of the CNRS National Institute of Physics (CIMI - ECHO - KEMTRONIX - PulSAr - VoltEdge - SAMSON). The PhD student will join the ECHO Team. This work is in the context of two projects ANR both
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minerals which precipitate at the interface between two grains enhance the mechanical properties of the porous media. We invite application for a PhD at the CNRS-University of Toulouse to gain a better
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genetically-induced rod degeneration and precipitates vision loss (Gegnaw et al, 2025). The PhD project aims at characterizing the mechanisms underlying this synergy by combining our mouse model of IRD (knock
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Polytechnique (Palaiseau) as part of the Advanced Microscopy team. The host team offers an interdisciplinary environment combining optics, computer science, and biology. The work will involve daily interactions
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global ocean model (ECCO-Darwin-type sediment module) to quantify alkalinity generation and associated CO2 storage. This PhD investigates the dissolution of calcium carbonate (CaCO3) in the deep sea, with
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competition between zones of advective transfer and zones of diffusive transfer where the fluxes of leaching reagents and products are very low. We invite application for a PhD at the CNRS-University
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2 Aug 2026 Job Information Organisation/Company CNRS Department Institut de Recherche sur les Archéomatériaux Research Field History History » Archaeology History » Medieval history Researcher Profile First Stage Researcher (R1) Application Deadline 22 Aug 2026 - 23:59 (UTC) Country France Type...
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number of undergraduate and graduate students—including many PhD candidates—as well as postdoctoral researchers and visiting scientists. The laboratory covers a wider range of topics than its name suggests
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at the glacier scale (Braconnot et al., 2019; Cretat et al., 2020). During this PhD, the candidate will study the relationships between high-altitude climate, geomorphological context, and glacier evolution during